Figure 7From: Imaging the hydrothermal system beneath the Jigokudani valley, Tateyama volcano, Japan: implications for structures controlling repeated phreatic eruptions from an audio-frequency magnetotelluric survey Results of the sensitivity test against a relatively conductive body (C3). (a) The resistivity of a region enclosed by the white dashed line was changed from the values of the best-fit model shown in the background to 200 Ωm. (b) Sounding curves obtained from the modified model (green line) are shown together with observed responses (red dots) and the best-fit curves (blue line). TM-mode apparent resistivity (upper) and phase (lower) for sites 02 (right) and 03 (left) are shown.Back to article page